Literature DB >> 23761231

Quantification of nitrogenase in Trichodesmium IMS 101: implications for iron limitation of nitrogen fixation in the ocean.

Sherrie Whittaker1, Kay D Bidle, Adam B Kustka, Paul G Falkowski.   

Abstract

Iron is widely thought to limit nitrogen fixation in the open, oligotrophic ocean due to the low solubility of Fe in oxic seawater and the high Fe demand for the nitrogenase holozyme. However, empirical evidence for Fe limitation of field populations of Trichodesmium based on either incubation experiments or molecular and physiological indicators has not quantitatively related Fe supply to the cellular Fe quotas for nitrogenase. Rather, the Fe required for N2 fixation has been inferred from in vivo catalytic activity. Using a pet14b expression vector, we cloned the nif H gene (encoding the Fe-protein, which contains 4Fe atoms per subunit) from Trichodesmium IMS 101, and purified the His-tagged apoprotein with which we derived a primary standard based on quantitative Western blots. Using a standard curve derived from the cloned Trichodesmium Fe apoprotein, we measured the absolute abundance of the Fe-protein in iron-replete cultures of this marine diazotroph. At peak expression, we calculate 0.04 mg nitrogenase mg(-1) C. Assuming a conservative stoichiometry of two Fe-protein subunits per MoFe protein (which contains 15 Fe atoms per subunit, or a total of 38 atoms of Fe per holozyme), we estimate 236 µmol Fe is bound to nitrogenase per mol cellular C. This estimate is about 10 times greater than the Fe previously calculated to support diazotrophic growth under these conditions. Our results suggest that under bloom conditions in the subtropical North Atlantic and North Pacific, as much as ∼2.22 and 0.06 µmol m(-3) of Fe is bound to Trichodesmium nitrogenase respectively. Such a high quota represents between ∼50% and > 100% summer-time average particulate Fe in surface waters, suggesting the importance of this taxon for the retention and biogeochemical cycling of Fe. Moderate growth (0.10 day(-1) ) towards the end of these blooms would require a vertical flux as high as ∼23 µmol Fe day(-1)  m(-2) into the mixed layer.
© 2010 Society for Applied Microbiology and Blackwell Publishing Ltd.

Entities:  

Year:  2011        PMID: 23761231     DOI: 10.1111/j.1758-2229.2010.00187.x

Source DB:  PubMed          Journal:  Environ Microbiol Rep        ISSN: 1758-2229            Impact factor:   3.541


  6 in total

1.  Outer Membrane Iron Uptake Pathways in the Model Cyanobacterium Synechocystis sp. Strain PCC 6803.

Authors:  Guo-Wei Qiu; Wen-Jing Lou; Chuan-Yu Sun; Nina Yang; Zheng-Ke Li; Ding-Lan Li; Sha-Sha Zang; Fei-Xue Fu; David A Hutchins; Hai-Bo Jiang; Bao-Sheng Qiu
Journal:  Appl Environ Microbiol       Date:  2018-09-17       Impact factor: 4.792

2.  The unique biogeochemical signature of the marine diazotroph trichodesmium.

Authors:  Jochen Nuester; Stefan Vogt; Matthew Newville; Adam B Kustka; Benjamin S Twining
Journal:  Front Microbiol       Date:  2012-04-26       Impact factor: 5.640

3.  Diel nitrogen fixation pattern of Trichodesmium: the interactive control of light and Ni.

Authors:  Irene B Rodriguez; Tung-Yuan Ho
Journal:  Sci Rep       Date:  2014-03-24       Impact factor: 4.379

Review 4.  Iron-Nutrient Interactions within Phytoplankton.

Authors:  Hanan Schoffman; Hagar Lis; Yeala Shaked; Nir Keren
Journal:  Front Plant Sci       Date:  2016-08-18       Impact factor: 5.753

5.  Abundances of iron-binding photosynthetic and nitrogen-fixing proteins of Trichodesmium both in culture and in situ from the North Atlantic.

Authors:  Sophie Richier; Anna I Macey; Nicola J Pratt; David J Honey; C Mark Moore; Thomas S Bibby
Journal:  PLoS One       Date:  2012-05-01       Impact factor: 3.240

Review 6.  Trichodesmium--a widespread marine cyanobacterium with unusual nitrogen fixation properties.

Authors:  Birgitta Bergman; Gustaf Sandh; Senjie Lin; John Larsson; Edward J Carpenter
Journal:  FEMS Microbiol Rev       Date:  2012-09-20       Impact factor: 16.408

  6 in total

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